Potassium (K) is the second most abundant nutrient element in plants after nitrogen (N), and has been shown to limit aboveground production in some contexts. However, the role of N and phosphorus (P) availability in mediating K limitation in terrestrial production remains poorly understood; and it is unknown whether K also limits belowground carbon (C) stocks, which contain at least three times more C than those aboveground stocks. By synthesizing 779 global paired observations (528, 125, and 126 for aboveground productivity, root biomass, and soil organic C [SOC], respectively), we found that K addition significantly increased aboveground production and SOC by 8% and 5%, respectively, but did not significantly affect root biomass (+9%). Moreover, enhanced N and/or P availability (through N and P addition) did not further amplify the positive effect of K on aboveground productivity. In other words, K had a positive effect on aboveground productivity only when N and/or P were limiting, indicating that K could somehow substitute for N or P when they were limiting. Climate variables mostly explained the variations in K effects; specifically, stronger positive responses of aboveground productivity and SOC to K were found in regions with high mean annual temperature and wetness. Our results suggest that K addition enhances C sequestration by increasing both aboveground productivity and SOC, contributing to climate mitigation, but the positive effects of K on terrestrial C stocks are not further amplified when N and P limitations are alleviated.
To assess the impact of the Laluo Hydropower Station on fish community structure and spawning habitat, hydraulic and ecological surveys were conducted in typical upstream and downstream of the station, and the physical biotopes distribution and fish community composition were obtained. By comparing the differences in fish community structure and spawning environment factors between the natural river sections and the downstream river section of the dam, analyse the impact of the station on the spawning grounds of fish in the downstream reaches of the dam and extract the main influencing factors. Results showed that the fish community in the study area is composed of Schizopygopsis younghusbandi, Schizothorox waltoni and Triplophysa spp., with S. younghusbandi being the dominant species. The physical biotopes of the spawning grounds for S. younghusbandi includes pools or glide, with a water depth of 0.3 ~ 1.0 m, flow velocity < 0.3 m/s and a substrate primarily consisting of fine particles such as sand and fine gravel. Downstream, the number of sexually mature individuals was low, with a skewed sex ratio, indicating significant spawning ground degradation. Water temperature, altered by the station's operation, was identified as the main factor disrupting spawning. This study contributes to the existing body of data and case studies in the field, advancing research on fish habitats in plateau rivers. It holds significant implications for the conservation of fish resources and the preservation of healthy aquatic ecosystems in these regions.
Soils are the largest terrestrial carbon sink on Earth, yet substantial uncertainty in the size and stability of this pool remains. Much of this uncertainty stems from the characterization of bulk density, which is the mass of a soil sample divided by its volume, a key property in the calculation of soil organic carbon (SOC) stocks. We used data from nearly 2900 plots in the United States (U.S.) Nationwide Forest Inventory to quantify SOC stocks in forests with three common methods of calculating soil bulk density. Mean SOC stocks calculated with these methods varied by up to 13 Mg ha−1, a difference equivalent to more than 70 percent of the 2022 economy-wide carbon dioxide emissions in the U.S. when scaled across all forest area. These differences were primarily driven by inconsistent treatment of coarse materials (i.e. rocks and roots) in soil bulk density calculations, which led to an overestimation of SOC content by 32 percent of the mean SOC stock across all U.S. forests. The largest discrepancies were found in soils with high coarse fragment content, which are more common in ecologically sensitive ecosystems like alpine zones and drylands, and in commercially important softwood forest types. Quantifying the size and stability of SOC in the land sector is essential to understanding how this carbon pool may serve as a nature-based solution to climate change. Consistent and transparent methods are necessary when estimating and reporting SOC content and when comparing SOC dynamics across ecological gradients, with disturbance, and over time.